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Exercises · 5.10

Q.Calculate the enthalpy change on freezing of 1.0 mol of water at 10.0 °C to ice at –10.0 °C. ΔfusH=6.03\Delta_{fus}H = 6.03 kJ mol−1^{-1} at 0 °C. Cp[H2O(l)]=75.3C_p[H_2O(l)] = 75.3 J mol−1^{-1} K−1^{-1}; Cp[H2O(s)]=36.8C_p[H_2O(s)] = 36.8 J mol−1^{-1} K−1^{-1}.

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The enthalpy change is found by breaking the process into three steps: cooling liquid water from 10 °C to 0 °C, freezing it at 0 °C, and cooling the resulting ice from 0 °C to –10 °C. The total is the sum of the enthalpy changes for each step, giving –6.25 kJ (rounded to three significant figures).

The problem asks for the enthalpy change when 1.0 mol of water freezes — but the water starts at 10 °C and the ice ends at –10 °C. You cannot simply use the enthalpy of fusion at 0 °C, because the temperature changes before and after freezing also carry enthalpy changes. The key insight: enthalpy is a state function, so we can design any convenient path that goes from the initial state (liquid, 10 °C) to the final state (solid, –10 °C) and sum the enthalpy changes along that path. The actual path doesn’t matter — only the start and end states do.

We choose a three‑step path:

  1. Cool the liquid water from 10 °C to 0 °C.
  2. Freeze the water at 0 °C (the reverse of fusion, so the sign flips).
  3. Cool the ice from 0 °C to –10 °C.

Each step uses the heat capacity or the enthalpy of phase change. Let’s work through them.


Step 1: Cooling liquid water from 10 °C to 0 °C

The enthalpy change for a temperature change at constant pressure is ΔH=nCpΔT\Delta H = n C_p \Delta T. Here n=1.0n = 1.0 mol, Cp(liquid)=75.3C_p(\text{liquid}) = 75.3 J mol⁻¹ K⁻¹, and ΔT=Tf−Ti=0−10=−10\Delta T = T_f - T_i = 0 - 10 = -10 K.

ΔH1=(1.0)(75.3)(−10)=−753 J=−0.753 kJ\Delta H_1 = (1.0)(75.3)(-10) = -753\ \text{J} = -0.753\ \text{kJ}

The negative sign makes sense: cooling releases heat, so enthalpy decreases.


Step 2: Freezing at 0 °C

The enthalpy of fusion (melting) is ΔfusH=+6.03\Delta_{fus}H = +6.03 kJ mol⁻¹. Freezing is the reverse process, so the enthalpy change for freezing is the negative of that:

ΔH2=−ΔfusH=−6.03 kJ\Delta H_2 = -\Delta_{fus}H = -6.03\ \text{kJ}

Again, negative because freezing is exothermic.


Step 3: Cooling ice from 0 °C to –10 °C

Now we use the heat capacity of solid water: Cp(solid)=36.8C_p(\text{solid}) = 36.8 J mol⁻¹ K⁻¹. The temperature change is ΔT=−10−0=−10\Delta T = -10 - 0 = -10 K.

ΔH3=(1.0)(36.8)(−10)=−368 J=−0.368 kJ\Delta H_3 = (1.0)(36.8)(-10) = -368\ \text{J} = -0.368\ \text{kJ} …

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